D.A.V. Stow
Abstract
Summary The Palaeozoic rocks of Hydra consist of a sequence of limestones and dolomites with some interbeds of shales and sandstones. Fusulinid foraminifera indicate the sequence is entirely Permian in age and not Carboniferous and Permian as previously thought.
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Summary The Palaeozoic rocks of Hydra consist of a sequence of limestones and dolomites with some interbeds of shales and sandstones. Fusulinid foraminifera indicate the sequence is entirely Permian in age and not Carboniferous and Permian as previously thought.
Key concepts: Permian, Paleozoic, Geology, Carboniferous, Paleontology, Lernaean Hydra, Foraminifera, Sequence (biology)